Niuchounei Pecten Fossil(牛稠內扇貝化石)
Most part of the mountain in Niuchounei are “half-faced”: one side is slope (inclining towards west), and the other side is a hanging cliff (east of the slope). The interbedding of mudstone and sandstone favors the formation of badlands. As the terrain inclines towards the west, meanders passing across cause lots of “half-faced” mountains, forming special landforms and landscapes.
Category Natural View